木栓質(zhì),木栓質(zhì)體,木栓質(zhì)煤素質(zhì)

The results of fluorescence evalution of cutinite and suberinite show th... 煤中角質(zhì)體和木栓質(zhì)體的光性演化表明其對本區(qū)煤成油有一定的貢獻(xiàn)。

Suberinite occurs commonly in Mesozoic coal measures and terrestrial organic matter source rocks in Northwest China, which is formed from suberized cell walls, particularly in plant periderm. 西北中生界煤系烴源巖中普遍含有木栓質(zhì)體，它來源于植物周皮的木栓化細(xì)胞壁。

Keywords Peat;Suberinite;Oxidation;Decomposition;Fluorescence; 泥炭;木栓質(zhì)體;氧化;分解;熒光;

Keywords suberinite;hydrocarbon generating evolution;thermal simulation experiment; 木栓質(zhì)體成烴演化熱;模擬實(shí)驗(yàn);

Keywords Coal measures;Oil source rock;Coal composition;Mesozoic era;Suberinite; 煤系;生油層;中生代;煤組分;木栓質(zhì)體;